1887
Volume 40 Number 4
  • E-ISSN: 1365-2478

Abstract

A

Seismic reflection data in the southern Gulf of Suez, offshore Egypt, are commonly severely affected by shallow velocity inhomogeneities in the form of diapiric salt bodies, and depth migration techniques must be used in order to image the presalt structure correctly. Frequently the diapir and the underlying prospective structure are three dimensional rather than two dimensional and thus require 3D techniques to resolve them. In addition, the severity of the problem is sometimes such that the common midpoint (CMP) stack assumptions are invalid and prestack depth migration is therefore required.

In 1990, Unocal developed a practical 3D prestack depth‐migration scheme, which was applied to a data set in the Gulf of Suez. The prospect was subsequently drilled and results proved the effectiveness of the technique.

This paper describes the use of the technique in the form of a case history. It is expected that the technique will be routinely used to solve similar problems.

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/content/journals/10.1111/j.1365-2478.1992.tb00533.x
2006-04-27
2024-04-26
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References

  1. Ball, G.1991. 3D Prestack Depth Migration of Seismic Data to Image Sub‐Salt Structure. In: Computer‐assisted Analysis and Modeling on the IBM 3090, H.U.Brown (ed.). MIT Press.
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  2. Guigon, I. and Frasson, F.1984. Geology of Egypt. In: Proceedings of Well Evaluation Conference, Egypt, C.M.Smith et al. (eds), 1–64. Schlumberger Middle East S.A.
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  3. Thiebaud, C.E. and Robson, D.A.1979. The geology of the area between Wadi Wardan and Wadi Gharandal, East Clysmic Rift, Sinai, Egypt. Journal of Petroleum Geology1, 63–75.
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  • Article Type: Research Article

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